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Oxygen isotopic determinations of sequentially erupted plagioclases in the 1974 magma of Fuego Volcano,Guatemala
Authors:W I Rose Jr  I Friedman  L G Woodruff
Institution:1. Michigan Technological University, 49931, Houghton, MI, USA
2. U. S. Geological Survey, 80225, Denver, CO, USA
3. Michigan Technological Univ., 49931, Houghton, MI, USA
Abstract:Plagioclases in the 1974 high-Al basalt from Fuego Volcano have δO18 values of +6.0 to +8.5 per mil. Meteoric water cannot have played a significant role in Fuego’s magma. Large, weakly zone clear phenocrysts had δO18 values in the accepted mantle range, while patchyzoned and oscillatory-zoned plagioclases inferred to have formed later and shallower levels have slightly heavier oxygen isotopic ratios.
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